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wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T...

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Page 1: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 2: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 3: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 4: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 5: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 6: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 7: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 8: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 9: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 10: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

Page 11: wopmay 300 dpi - ucalgary.ca · in an effort to develop practical methods of inferring the P —T conditions of metamorphosed rocks (geothermometry and geobarometry). Examples of

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